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EARTH`S FORMATION AND STRUCTURE The earth formed
EARTH`S FORMATION AND STRUCTURE The earth formed

... Eventually, bodies of several kilometers in diameter formed; these are known as planetesimals. The largest planetesimals grew fastest, at the expense of the smaller ones. This process continued until an earth-sized planet had formed. Early in its formation, the earth must have been completely molten ...
Earth Science
Earth Science

... pieces of continental and oceanic crust. 13. The theory that pieces of Earth’s lithosphere are in constant motion, driven by convection currents in the mantle. 14. Vibrations that travel through Earth carrying the energy released during an earthquake. 15. The movement of a fluids caused by differenc ...
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Science 7

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general_science_syllabus

... Explain how the outward transfer of Earth’s internal heat drives the convection circulation in the mantle to move tectonic plates. ...
Ch 5 wo cycles
Ch 5 wo cycles

... warming the planet to a habitable temp powers the biogeochemical cycles allows producers to photosynthesize and feed other living organisms ...
PPT
PPT

... disk-shaped cloud of gas and dust. protostar rocky volatile ...
Earth`s Layered Interior - Donovan
Earth`s Layered Interior - Donovan

... o Heat rises to the surface, cools and drops back down  2,800 km in thickness and varies in temperature  boundary between crust and mantle is known as the MOHO or the Mohorovicic Discontinuity named after a Croatian seismologist who discovered it The Core  The Core is divided into 2 parts – inner ...
Earth`s Interior - Union Beach School District
Earth`s Interior - Union Beach School District

... » The inner core of the Earth has temperatures and pressures so great that the metals are squeezed together and are not able to move about like a liquid, but are forced to vibrate in place like a solid. » 1200 km thick ...
Deadly quakes help renew the planet
Deadly quakes help renew the planet

... they admire has just caused a staggering loss of life. Even so, scientists argue that in the very long view, the global process behind great earthquakes is quite advantageous for life on Earth — especially human life. Powerful jolts like the one off Sumatra on Dec. 26 that sent massive waves racing ...
Guided Reading on Sections 23.3 and 23.4
Guided Reading on Sections 23.3 and 23.4

... the planet resulted in its ___________________, which caused the outer skin to contort and wrinkle into ____________________ and ________________. 3. Many people had noticed, however, that the eastern shorelines of ___________ __________________ and the western shoreline of ______________ seemed to ...
Linking Asteroids and Meteorites through Reflectance
Linking Asteroids and Meteorites through Reflectance

... • If you can see rocks on the surface that comes from the interior, you can study them ...
PowerPoint Presentation - Introduction to Earthquakes EASA
PowerPoint Presentation - Introduction to Earthquakes EASA

... How does Oceanic Crust differ from Continental Crust? ___________________________________________________________________________ ___________________________________________________________________________ ___________________________________________________________________________ ...
High-Performance Modelling in Geodynamics
High-Performance Modelling in Geodynamics

... This title is available in InfoSci-Books, InfoSci-Software Technologies, Science, Engineering, and Information Technology, InfoSci-Computer Science and Information Technology, InfoSci-Select, InfoSci-Select. Recommend this product to your librarian: www.igi-global.com/e-resources/library-recommendat ...
SCI Ch2 Study Guide KEY
SCI Ch2 Study Guide KEY

... Erosion is the process that wears away soil and rock. Erosion can be caused by water, wind, ice, and gravity. An example of erosion is rivers and streams carrying rock fragments as the water flows downhill. 3. How are U-shaped valleys formed? ...
Chapter 1, Section 1 – Earth`s Interior
Chapter 1, Section 1 – Earth`s Interior

... c. Lower mantle: solid material that extends to core iii. Core: innermost layer of mantle 1. made of iron and nickel 2. two parts: a. liquid (molten metal) outer core b. solid metal inner core (under too much pressure for iron and nickel molecules to spread out) b. Core and magnetic field i. Created ...
Earth`s Interior Information- Core-Innermost layer Inner Core
Earth`s Interior Information- Core-Innermost layer Inner Core

... Asthenosphere-Not liquid, but there is melted rock, carries the lithosphere, moves slowly Lithosphere-broken into giant plates that fit around the globe like puzzle pieces. The pieces move a little bit each year. They slide on a somewhat liquid asthenosphere Crust-Layer of rock that forms Earth’s ou ...
The Earth Guiding Questions Minerals Telling Rocks Apart • How
The Earth Guiding Questions Minerals Telling Rocks Apart • How

... Guiding Questions The Earth 1. What is the greenhouse effect? How does it affect the average temperature of the Earth? 2. Is the Earth completely solid inside? How can scientists tell? 3. How is it possible for entire continents to move across the face of the Earth? 4. How does our planet’s magnetic ...
The Earths Crust Quick Key
The Earths Crust Quick Key

... Completely fill in each circle with a black pen, making sure you do not go outside. Make sure the fill in your name and Student ID on the answer key. 1. How many layers make up the Earth? A ...
: 3.8 MB - Okala Practitioner
: 3.8 MB - Okala Practitioner

... The  biosphere  is  unique  in  the  universe.  No  other  living  planets  have  yet   been  found.  The  biosphere  evolved  over  a  rather  incomprehensible   period  of  five  billion  years.     ...
Q-gameHow are winds named
Q-gameHow are winds named

... 112.The type of fossil that is like a hole, a hollow area left behind by an organism that decomposed later is called a/n______? 113.The times that day & night are of equal length are the _______. 114.Galileo called the dark, flat parts of the moon ______. 115.What do you call a meteoroid that hits E ...
Introduction to geology
Introduction to geology

... *The Paleo -atmosphere was Free of Oxygen. *Blue- algae uni-cell played a good role for supply the atmosphere by a free Oxygen. Which is an important for organisms life. 2- Cooling processes:* Cooling processes leads to:* condensation of water vapor in the atmosphere, and then leaks and infiltrate t ...
chart_set_5
chart_set_5

... Other side has weaker pull => bulges away compared to rest of Earth. The Earth spins once a day while the bulge always points towards and away from the Moon => high and low tides. We also see tidal forces at work in other places in the Universe. ...
#______ Parent Signature: Heading: The Earth`s Changing Surface
#______ Parent Signature: Heading: The Earth`s Changing Surface

... o Answer the questions below in complete sentences where appropriate. 1. Which of the following are examples of constructive forces? A. Volcanoes, mountain/island building, and deposition B. Earthquakes, weathering, and erosion C. Tornadoes, hurricanes, volcanoes D. Earthquakes, tidal waves, erosion ...
6th grade Science Unit 1.3 Structures of the Earth and Energy
6th grade Science Unit 1.3 Structures of the Earth and Energy

... My learning targets: 6.7 Matter and energy. The student knows that some of Earth's energy resources are available on a nearly perpetual basis, while others can be renewed over a relatively short period of time. Some energy resources, once depleted, are essentially nonrenewable. 6.10 Earth and space. ...
LAYERS OF THE EARTH
LAYERS OF THE EARTH

... crust) to 25 miles (continental crust). The crust is more dense under the ocean and less dense under the continents. The oceanic crust is mostly composed of basalt. The continental crust is mainly made of granite. The crust temperature is up to 930 degrees Farenheit. 3. asthenosphere – the layer of ...
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